In a homogeneous ambient fluid, and is constant. Use kinematic fluxes or, equivalently, the primitive form of the unsteady top-hat line-plume balances:
Here is the positive buoyant reduced gravity. Seek a nonsteady separable power-law ansatz with both time differentiation and vertical transport retained. Matching powers in the volume equation forces with no time dependence. Matching the two momentum terms then gives , and the buoyancy force has , where is a shifted age. Thus write
Substitution determines the constants rather than just the exponents. The volume equation gives , so for a nonzero buoyant plume . The momentum equation gives , while the buoyancy equation gives . The buoyant nontrivial branch has and . Consequently the separable decaying top-hat line plume is
The Boussinesq approximation requires . The corresponding mass density-weighted fluxes, to this order, are
For a direct check, is time independent and . Hence , , and . This verifies all three balances and the required width coefficient.
This nonsteady branch is not the steady, continuously supplied, constant-flux line plume. The latter has constant and half-width in the same top-hat convention. Also, the unshifted power law has as and is singular at . It is therefore an interior separable solution, not by itself a solution with a nonzero continuously operating point-source flux at the origin. A finite-width source boundary, a virtual origin, or a matching region is needed to connect it to physical source and initial data. For example, replacing by supplies a finite base width and time-varying positive base fluxes when . No source or initial flux history is specified in the question to select that matching; the requested power-law width follows from the local balances above.